Specific gravity (Gs) is a dimensionless property that compares the density of soil solids to the density of water at 4β―Β°C, providing insight into the mineral composition and void ratio of the soil.
In the laboratory, Gs is obtained by measuring the weight of a dry soil sample in air (Ws) and its apparent weight when submerged in water (Ww). The difference between these weights represents the buoyant force, which is directly related to the volume of the soil solids.
Ws = weight of soil in air (g)
Ww = weight of soil in water (g)
A typical Gs value for siliceous sands ranges from 2.60 to 2.70, whereas organic clays may exhibit values as low as 2.30. Accurate determination of Gs is essential for converting between weight and volume in geotechnical analyses such as settlement and bearing capacity calculations.
What is specific gravity in soil?
How do I measure weight in air for soil?
What does apparent weight in water mean?
How do I calculate specific gravity from weights?
Why is 4Β°C used for water density?
What does specific gravity tell us about soil?
Can I use this calculator with any type of soil?
Results are for informational purposes only and do not constitute professional advice.
